Talcott Mountain of central Connecticut, with a high point of 950 feet (290 m), is a 13-mile (21 km) long trap rock mountain ridge located 6 miles (10 km) west of the city of Hartford. The ridge, a prominent landscape feature, forms a continuous line of exposed western cliffs visible across the Farmington River valley from Farmington to Simsbury. Talcott Mountain is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.
A popular outdoor recreation resource, Talcott Mountain is known for its microclimate ecosystems, rare plant communities, and expansive views from cliffs that tower up to 700 ft (213 m) above the surrounding landscape.
Talcott Mountain encompasses two state parks, several municipal recreation areas and reservoirs, a science center and school, a demonstration forest, and the historic Heublein Tower. The 51-mile (82 km) Metacomet Trail traverses the ridge.
Read more about Talcott Mountain: Geography, Geology, Ecosystem, Recreation, Conservation and Education, See Also
Famous quotes containing the word mountain:
“We noticed several other sandy tracts in our voyage; and the course of the Merrimack can be traced from the nearest mountain by its yellow sand-banks, though the river itself is for the most part invisible. Lawsuits, as we hear, have in some cases grown out of these causes. Railroads have been made through certain irritable districts, breaking their sod, and so have set the sand to blowing, till it has converted fertile farms into deserts, and the company has had to pay the damages.”
—Henry David Thoreau (1817–1862)